Proceedings of the International Congress of Mathematicians August 16-24, 1983, Warszawa SEEGITJ KLATNEEMAE" Long Time Behaviour of Solutions to Nonlinear Wave Equations Most basic equations of both, physics and geometry have the form of nonlinear, second order, autonomous systems G(u,u',u") = 0, (1) 1 2 n+1 where u = u(x , x ,..., x ), and u', u" denote all the first and second partial derivatives of u. For simplicity we will assume here that both u and G are scalars and denote by ua, uab, the partial derivatives dau and respectively d2ahu; a,b =1,2, ..., n+1. Let uQ(x) be a given solution of (1). Our equation is said to be elliptic or hyperbolic at u°(x) according to whether the (n+l)x(n+^l) matrix, whose entries are Gab = --—(u°9 u0', u°"), is nondegenerate and has signature (1,...,1,1) or (1,..., 1, —1). Nonlinear elliptic equations and systems have received a lot of attention in the past forty or fifty years and in this period a lot of progress was made and powerful methods were developed. By comparison, the field of nonlinear hyperbolic equations is wide open. In what follows I will try to point out some recent developments concerning long-time behaviour of smooth solutions to a large class of such equations. Let us assume that (7(0, 0,0) = 0 and that (1) is hyperbolic around the trivial solution u° = 0. Typically, the operator obtained by linearizing (1) around u° H== 0 contains only second derivatives. Without further loss of generality we may assume it to be the wave operator d\ + . . . + d2n — d) = — D9 where we have ascribed to xn+1 the role of the time variable t. The equation (1) takes the form (1') nu =I?(u9u',u") (!') n with F a smooth function of (u,u',u ), independent of uu, vanishing together with all its first derivatives at (0,0, 0). [1209] 1210 Section 11: S. KLainerman Associate to (1') the pure initial value problem u(x, 0) = sf(x), ut(x, 0) = sg(x) y (l'a) with/, g, ö°°-functions, decaying sufficiently fast at infinity (for simplicity, sa y ft 9 eG™(Rn)) and e is a parameter which measures the amplitude of the data. Given /, g and F we define the life span Î7* = T#(e) as the supremum over all T > 0 such that a <7°°-solution of (1'), (l'a) exists for all xeRn, 0 < £ < J F . The fundamental local existence theorem ([3], [4], [14], [24], [27]), asserts that, if s is sufficiently small, so that the initial data lies in a neighborhood of hyperbolicity of the zero solution, then T*(s) > 0. Moreover, a simple analysis of the proof shows that T*(e) > A — 8 where A is some small constant, depending only on a finite number of derivatives of Fr f, g. This lower bound for 2% is in general sharp if the number of space dimensions n is equal to one. Indeed let our variables in (1') be x and t and F = o,(%)^œa. with a a smooth function, <r(0) = 0. An old result of P. Lax [22], extended to systems of wave equations by F. John [10], shows that, under the assumption of "genuine nonlinearity", (/(O) ^ 0, all solutions to the corresponding initial value problem (l'a) blow up by the time O (—). Eecently, in [20], it was proved that 2* < oo even if the genuine nonlinearity condition is violated. More precisely, assume that <r'(0) = ... = or(p)(0) = 0, a(p+1)(0) ^ 0 then the corresponding solutions blow up by the time T = 0(1 /e**4"1). In both situations the blow-up occurs in the second derivatives of u i.e. uxx becomes infinite while ut, ux remain bounded. Such blow-ups are typical of shock formations and are observable phenomena of physical reality. If the original equation, or system can be written in conservation form i.e., in our case, F(u9u',un) n+l = ]? dafa(u,u'), one can try to^exteiM the solutions past a=l these breakdown points by introducing the concept of weak solutions. This was successfully accomplished for very general first order systems of conservation laws, in one space dimension, by the fundamental work of Oleinik, P. Lax and J. Glimm (see [24] for a bibliography). In this lecture I will restrict myself, however, to classical, i.e. 0°°-solutions. Suprisingly, the situation looks better in higher dimensions. In 1976 F. John [9] proved that, under the assumption F = F(u', u"), and n^39 T*(s) can be significantly improved and, in 1980, S. Klainerman [15] was able to push T*(e) to infinity, and thus obtain global solutions, provided that n^Q. More generally, see ([17], [21], [38]), Long Time Behavionr of Solutions to Nonlinear Wave Equations 1211 1. Assitme that F = F(u',u") = 0(\u'\ + \u"\Y+l for 1/ 1\ n-1 uf, u" and that—I1H J< , then there exists an e0 sufficiently small THEOKEM such that for all e < £ 0 , (1'), (l'a) has a unique smooth solution for all x G Rn, t ^ 0.1 The reason for this improved behaviour of solutions of (1') in higher dimensions was beautifully illustrated by F . John [9] with the following quotation from Shakespeare, Henry VI: "Glory is like a circle in the water, Which never ceaseth to enlarge itself, Till by broad spreading it disperse to naught". Indeed, the higher the dimension the more room for waves to disperse and thus decay. Accordingly, the key to [9], [15], [17], [21] and [28] is to use decay estimates for solutions to the classical wave equation, • u = 0 (see [25], [26], [31]), and to combine them with energy estimates for higher derivatives of solutions to the original, nonlinear equations. The dimension n = 3, which nature gives preference, is not only the most important but also the most challenging. In [7] F . John exhibited an example for which T* < oo. More precisely consider F = ut-uu and the corresponding equation (1') in three space dimensions. Imposing only one mild restriction on the data, jg(x)dx > 0, F . John showed that there are no C2-solutions defined for all x e fi3, t ^ 0. However, for sufficiently small s, the solutions remain smooth for an extremely long-time before a breakdown occurs. We have in fact the following very general. THEOKEM 2 (F. John, S. Klainerman). Assume that F verifies one of the following hypothesis : (Hx) F does not depend explicitly on u i.e., F = F(u', u") (H2) F can be written in conservation form, 4 0=1 (R'2) F(u, u', u") = V 8Ja(u, «0 +0(\u\ + \u'\ + \u"\)3 for small u, u',u 1 The author was recently able to improve this result [32]. The sharp condition which assures global existence is p > 2j(n — 1). 1212 Section 11: S, Klainerman Then, there exist three small, positive constcmts eö, A9 depending only on a finite number of derivatives of F9 /, g, such that for every 0 < s < s09 T*( ß )>exp(A/s). Previously a weaker, polynomially long time existence result, was proved by F. John in [12] using an asymptotic expansion in powers of s, for u (see also [9]). The exponential long-time existence result was first proved, for spherically symmetric solutions (in the semilinear case F = F(u'), by F. John [7] and T. Sideris [29], and for F = F(u'9 u") by S. Klainerman [18]). The result of Theorem 2 is in general sharp. Indeed, F. John [11] proved recently that this is the case in the context of his previous example, F = utuu. There is, however, quite a rich class of nonlinearities F for which global existence holds. The following can be regarded as a generalization of Theorem 1 in dimension n = 3. TEGEOKEM 3. Assume that F verifies the following "Null"-condition P) 2 J^(u9u99u9')JPJ? = 0(\u\+ \u'\ + \u"\?9 ( ü ). 2 ^ 0 „ 6c («,«',«")X"z 6 x c = O(|«I + I«'I+I«"I)', a,b,c=l (iii) j ; KabUJu,u%u")XaXbX°X*=0(\ul + \u'\ + \u"\)3 (ISO for every sufficiently small u9 u', u" and any fixed null space-time vector (JP,Z«, J 3 ,X*) i.e., (Z1)" + (Z")» + (Z8)»-(2:*)" = 0 . Then, if e is sufficiently small, a global smooth solution of (!'), (l'a) To illustrate the content of Theorem 2 note that either of the following examples verifies the condition (N) Example 1 F = uaubc — ubuac9 for any three indices a9 6, c = 1, 2, 3, 4 Example 2 F = da(u2 — u\ — u\--u\)9 for any index a = 1 , 2 , 3 , 4 . The proof of both Theorems 2 and 3 depends on some recent [19] weighted L°° and L1 estimates for solutions to the classical, inhomogeneous, wave equation in dimension n = 3. They were first used, in the spherical symmetric case, in [18] and then extended to the general case by introducing the angular momentum operators Qx = x3d2—x%d39 Q2 =^x1d3 — — x3d19 Qs = xzd1 — x1dz. Their key property is that they commute with the wave operator • and thus can be treated as the usual partial deriva- Long Time Behaviour of Solutions to Nonlinear Wave Equations 1213 tives d19 d2, da. In particular, this allows us to extend the energy estimates used in [9], [15], [17], [21] and [28], to any combination of the derivatives ^u 5 2 , d3, Q19 Q2, P3. The operators Q19 Q2, AJ are closely connected to t h e "radiation operators" Z19 L29 L3 which played a fundamental role m [12]. A different, and very interesting proof of Theorem 3, based on some conformai mapping methods, was given by D. Christodoulou [1], (See also his previous joint work with T. Ohoquet-Bruhat [2].) Both Theorems 2 and 3 have straightforward extensions to systems, in particular to those of the type arising in Nonlinear Elasticity and General Eelativity. There are important problems, like that of stability of the Minkowski Space as a solution of the Einstein equations in vacuum, for which we hope that Theorems 2 and 3 could be relèvent. In the scalar case we believe that the picture provided by these theorems, together with the nonexistence results of F. John [7], [11] can be completed. In other words, we conjecture that if one of the hypothesis (HI), (H2), (H2') holds and (N) fails, then the lower bound on T*(e) given by Theorem 2 is sharp, i.e. singularities must develop by that time, for any choice of / or g and e small. An important open question is to describe the type of blow-up which occurs in that case. If JP is quasilinear and verifies H I , we expect that, as for n =1, the breakdown occurs when the second derivatives of u become infinite while the first derivatives remain bounded. The recent work of F. John [28] points in this direction, but completely satisfactory results are still missing. Another open question is to derive results similar to Theorems 2 and 3 for the dimensions n = 2 and n = 4. We suspect that the corresponding, optimal lower bound for I7* for n = 2 must be 01 — J while for n *= 4 one should be able to prove global existence.2 I n this respect we hope to find decay estimates similar to those of [19] for n T^ 3. The same type of questions can be asked for equations (1') where the wave operator Q is replaced by the Klein-Gordon operator, \J + m2 or the Schrödinger operator —id(+A. General results of the type of Theorem 1 were derived in [17], [21], [28], and for nonlinearities depending only on u in [30], (see also the reference there). The methods used to derive Theorems 2 and 3 might be used to substantially improve these results. I n the end, I like to apologize for not mentioning the work of many 2 See footnote, p. 1211. 1214 Section 1 1 : S. Klainerman other authors. I n particular I have left out a lot of interesting results concerning semilinear equations i.e. F = F(u) in (l') f For an up to date bibliography concerning such results I refer to the recent papers of E. Glassey [5],, [6]. r References [1] Christodoulou D., Global Existence to Nonlinear Wave liquations, in preparation. [2] Choquet-Bruhat Y. and Christodoulou D., Existence of Global Solutions of the Yang-Mills, Higgs Fields in 4-Dimensional Minkowski Space, I, I I , Comm. Math. Physics 83 (1982), p p . 171-191, pp. 193-212. [3] Courant E., Friederichs K. 0 . and Lewy H., Über die partiellen Differentialgleichungen der mathematischen Physik. Math. Annalen 100 (1928), pp. 32-74. [4] Friederichs K. 0., Symmetrie Hyperbolic Linear Differential Equations, Comm. Pure Appi. Math. 7 (1954), pp. 345-392. [5] Glassey R., Existence in the Large for n w — F(u) in Two Space Dimensions Math., Z. 178 (1981), p p . 233-261. [6] Glassey R., Finite Time Blow-Up for Solutions of Wonlinear Wave Equations, Math. Z. 177 (1981), p p . 323-340. [7] John F . , Blow-up for Quasilinear Wave Equations in Three Space Dimensions, Gomm. Pure Appi. Math. 34 (1981), pp. 29-51. BF (ut) [8] John F., Blow-up of Badial Solutions of Hu — , in preparation. but [9] John F . , Delayed Singularity Formation in Solutions of Nonlinear Wave Equations in Higher Dimensions, Oomm. Pure Appi. Math. 29 (1976), pp. 649-681. [10] John F . , Formation of Singularities in One-Dimensional Nonlinear Wave Propagation, Oomm. Pure Appi. Math. 27 (1974), pp. 377-405. [11] John F., Improved Estimates for Blow-up for Solutions of Strictly Hyperbolie Equations in Three Space Dimensions, in preparation. [12] John F., Lower Bounds for the Life-Span of Solutions of Nonlinear Wave Equations in Three Space Dimensions, to appear in Comm. Pure Appi. Math., 1983. [13] J o h n F . , Klainerman S., Almost Global Existence to Nonlinear Wave Equations in Three Space Dimensions, O.P.A.M, 1984. [14] Kato T., Linear and Quasilinear Equations of Evolution of Hyperbolie Type, C.I.M.E. I I CICLO, 1976. [15] Klainerman S., Global Existence for Nonlinear Wave Equations, Oomm. Pure Appi. Math. 33 (1980), p p . 43-101. [16] Klainerman S., Global Existence to Nonlinear Wave Equations in Three Space Dimensions, in preparation. [17] Klainerman S., Long-Time Behaviour of Solutions to Nonlinear Evolution Equations, Arch. Bat. Mech. and Anal. 78 (1982), pp. 73-98. [18] Klainerman S. On Almost Global Existence to Nonlinear Wave Equations in Three Space Dimensions, to appear in Oomm. Pure Appi. Math., 1983. [19] Klainerman S., Weighted L°° and L1 Estimates for Solutions to the Equation in Three Dimensions, to appear in Oomm. Pure Appi. Math., 1984. Long Time Behaviour of Solutions to Nonlinear Wave Equations 1215 [20] Klainerman S. and Majda A., Formation of Singularities for Wave Equations Including the Nonlinear Vibrating String, Oomm. Pure Appi. Math. 33 (1980), p p . 241-263. [21] Klainerman S. and Ponce G., Global Small Amplitude Solutions to Nonlinear Evolution Equations, Oomm. Pure Appi. Math. 36 (1983), p p . 133-141. [22] Lax P . D., Development of Singularities of Solutions of Nonlinear Hyperbolic Partial Differential Equations, J. Math. Phys. 5 (1964), p p . 611-613. [23] Lax P., Hyperbolic Systems of Conservation Laws and the Mathematical Theory of Shock Waves, 0. B . M. S., Monograph No. 11, SIAM, 1973. [24] Leray J., Hyperbolic Differential Equations, Princeton, 1952. [25] Marshall B., Strauss W. and Wainger S., Lp — LQ Estimates for the Klein-Gordon Equation, J. Math. Pure Appi. 59 (1980), pp. 417-440. [26] Pécher H., If-Abschätzungen und klassische Lösungen für nichtlineare Wellengleichungen, Math. Z. 150 (1976), pp. 159-183. [27] Schauder J., Das Anfangswertproblem einer quasilinearen hyperbolischen Differentialgleichung zweiter Ordnung in beliebiger Anzahl von unabhängigen Veränderlichen, Fundamenta Mathematicae 24 (1935), pp. 213-246. [28] Shatah J., Global Existence of Small Solutions to Nonlinear Evolution Equations, preprint. [29] Sideris T., Global Behaviour of Solutions to Nonlinear Wave Equations in Three Space Dimensions, preprint, 1982. [30] Strauss W., Nonlinear Scattering Theory of low energy, J. Funct. Anal. 41 (1981), pp. 110-133. [31] Von Wahl W., Z/^-Decay Rates for Homogeneous Wave Equations, Math. A., 120 (1971), pp. 93-106. Added in proof. [32] Klainerman S., Apriori Uniform Decay Estimates for Solutions of the Classical Wave Equation and Applications to Nonlinear Problems, preprint.
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